The term "Bermuda High" refers to a semi-permanent high-pressure system located in the Bermuda region of the North Atlantic Ocean. This weather phenomenon typically influences the climate and weather patterns in the eastern United States and parts of the Caribbean. It is characterized by warm, dry air and can lead to calm seas and sunny weather. The Bermuda High plays a significant role in the formation of tropical storms and hurricanes. When it is strong, it can steer these storms away from the U.S. mainland, while a weaker Bermuda High may allow storms to move closer to land, impacting coastal areas.